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P010010-00-R - LIGO - California Institute of Technology

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1.3 Interferometer Sensitivity<br />

5<br />

Concurrent with the construction <strong>of</strong> the first generation <strong>LIGO</strong> detector (<strong>LIGO</strong> I) is the<br />

work <strong>of</strong> an international collaboration, the <strong>LIGO</strong> Scientific Collaboration (LSC), to<br />

develop the next generation interferometer, <strong>LIGO</strong> II.[12] The planned improvements<br />

lead to nearly an order <strong>of</strong> magnitude increase in the sensitivity across the bandwidth,<br />

as well as extending the bandwidth to lower frequencies. To understand how this is<br />

to be accomplished requires some description <strong>of</strong> the limits to the sensitivity <strong>of</strong> the<br />

detector, and how that sensitivity is shaped. In brief, the sensitivity is defined by the<br />

noise which limits the measurement (seismic, thermal, and shot noise), as well as the<br />

gain <strong>of</strong> the interferometer. <strong>LIGO</strong> II will use improved technology and materials to<br />

reduce the noise due to seismic and thermal noise. Increased laser power will reduce<br />

shot noise. An advanced interferometer configuration will shift the maximum gain <strong>of</strong><br />

the detector away from DC into the bandwidth <strong>of</strong> interest by placing a mirror at the<br />

output, similar to the original GEO6<strong>00</strong> interferometer. This will generally be referred<br />

to as a signal tuned interferometer.<br />

1.3.1 Seismic Noise<br />

The measurement <strong>of</strong> the gravitational wave is accomplished by monitoring the relative<br />

distance between the surfaces <strong>of</strong> two test masses. Any other force which disturbs the<br />

center <strong>of</strong> mass or the surface <strong>of</strong> the mass itself makes the measurement ambiguous – it<br />

is unclear whether the disturbance is due to the gravitational wave or the noise force.<br />

A ground-based interferometer must be, at some level, mechanically coupled to the<br />

earth, hence the masses are subject to seismically driven vibrations. The dominant<br />

part <strong>of</strong> the seismic power spectrum is at low frequencies. This varies, sometimes by<br />

an order <strong>of</strong> magnitude or more around the world, but a moderately quiet site will<br />

have a spectrum <strong>of</strong> roughly x(f) = 10 −8 m/ √ Hz × (1Hz/f) 2 .<br />

Techniques for reducing the effects <strong>of</strong> seismic noise have long been known, and yet<br />

new designs and approaches continue to improve vibration isolation. Two different<br />

approaches have been taken: passive and active.

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